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JOURNAL OF DESERT RESEARCH  2013, Vol. 33 Issue (2): 358-366    DOI: 10.7522/j.issn.1000-694X.2013.00050
Biology and Soil     
Vegetation Degradation and Its Correlation with Rainfall Interception and Soil in Rocky Desertification Area of Northern Guangdong
LU Guan-yao1,2, WEI Xing-hu2, LI Sen1, XIONG Yan2, LEI Li3
1.Department of Geographic and Environmental Science,Northwest Normal University, Lanzhou 730070, China;
2.Resources and Environmental Science Research Institute, Foshan University, Foshan 528000, China;
3.School of Geography, South China Normal University, Guangzhou 510631, China
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Abstract  

We studied the vegetation degradation and its correlation with rainfall interception and soil in rocky desertification area of northern Guangdong with methods of site investigation, station-oriented observation and simulated test. The results showed that: In accordance to the light, middle, severe and extremely severe rocky desertificaiton, the plant community succession was from Herb+liana+shrub+Arbor to herb to bryophyta, the community's layer was from 4 layers to 4 layers to 2 layers to 1 layer; the average height was from 87.06 cm to 63.32 cm to 42.13 cm to 6.21 cm; proportion of species reduction was from 0% to14% to 46% to 86%; the dominant species of plants were from Pistacia chinensis+Boehmeria nivea+Vitex negundo+Pueraria phaseoloides to Pistacia chinensis+Artemisia apiacea+Chrysanthemum indicum to Miscanthus floridulu+Arundinella anomala+Eleusine indica to bryophyta; the Margalef index was from 2.33 to 2 to 1.25 to 0.33; the Shannon-Wiener index was from 2.96 to 2.31 to 1.94 to 0.42. There is a significant correlation both between vegetation degradation and rainfall and between vegetation degradation and soil.

Key words:  rocky desertification      vegetation degradation      rainfall      soil      northern Guangdong     
Received:  25 September 2012      Published:  29 October 2012
ZTFLH:  Q948  

Cite this article: 

LU Guan-yao1,2, WEI Xing-hu2, LI Sen1, XIONG Yan2, LEI Li3. Vegetation Degradation and Its Correlation with Rainfall Interception and Soil in Rocky Desertification Area of Northern Guangdong. JOURNAL OF DESERT RESEARCH, 2013, 33(2): 358-366.

URL: 

http://www.desert.ac.cn/EN/10.7522/j.issn.1000-694X.2013.00050     OR     http://www.desert.ac.cn/EN/Y2013/V33/I2/358

[1]李森,董玉祥,王金华.土地石漠化概念与分级问题再探讨[J].中国岩溶,2007,26(4):279-284.



[2]朱守谦,陈正仁,魏鲁明.退化喀斯特森林自然恢复的过程和格局[J].贵州大学学报,2002,21(1):19-25.



[3]李森,魏兴琥,张素红,等.典型岩溶山区土地石漠化过程——以粤北岩溶山区为例[J].生态学报,2010,30(3):674-684.



[4]蔡道雄,卢立华.浅谈石漠化治理的对策及造林技术措施[J].世界林业研究,2002,15(2):76-80.



[5]黄树鹏,陆魏峰,曾土荣,等.粤北岩溶石山地区地下水资源勘查与生态环境地质调查报告[R].广州:广东省地质调查院,2002.



[6]李森,魏兴琥,黄金国,等.中国南方岩溶区土地石漠化的成因与过程[J].中国沙漠,2007,27(6):918-926.



[7]王兮之,李森,王金华.粤北典型岩溶山区土地石漠化景观格局动态分析[J].中国沙漠,2007,27(5):758-764.



[8]王金华,李森,李辉霞,等.石漠化土地分级指征及其遥感影像特征分析——以粤北岩溶山区为例[J].中国沙漠,2007,27(5):765-770.



[9]黄金国.粤北岩溶山区水土流失现状与治理对策[J].水土保持研究,2007,14(5):73-75.



[10]黄金国,李森,魏兴琥.粤北岩溶山区土地石漠化治理与农业综合开发模式研究[J].中国沙漠,2008,28(1):39-43.



[11]王明刚,李森.粤北石漠化地区坡地土壤侵蚀模拟试验研究[J].中国沙漠,2011,31(6):1488-1492.



[12]魏兴琥,陆冠尧,周红艳,等.粤北石漠化灌丛坡地模拟降雨地表径流水中钙离子含量变化[J].中国沙漠,2011,31(5):1343-1347.



[13]黄金国,李森,魏兴琥,等.粤北岩溶山区石漠化过程中土壤养分变化研究[J].中国沙漠,2012,32(1):163-167.



[14]Magurran A E. Ecological Diversity and Its Measurement[M].New Jersy:Princeton University Press,1988.

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